On the variability of the quarter-diurnal tide in the MLT over Brazilian low-latitude stations

Abstract The characteristic features of the quarterdiurnal tide (QDT) in the mesosphere and lower thermosphere (MLT) are investigated using meteor radar observations from three low-latitude southern hemispheric stations, Sao Joao do Cariri (7.4°S, 36.5°W), Cachoeira Paulista (22.7°S, 45°W) and Santa...

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Main Authors: Amitava Guharay, Paulo Prado Batista, Ricardo Arlen Buriti, Nelson Jorge Schuch
Format: Article
Language:English
Published: SpringerOpen 2018-08-01
Series:Earth, Planets and Space
Subjects:
Online Access:http://link.springer.com/article/10.1186/s40623-018-0910-9
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spelling doaj-02232dcfb1534e568aa4d91d0426a4952020-11-25T01:40:09ZengSpringerOpenEarth, Planets and Space1880-59812018-08-0170111410.1186/s40623-018-0910-9On the variability of the quarter-diurnal tide in the MLT over Brazilian low-latitude stationsAmitava Guharay0Paulo Prado Batista1Ricardo Arlen Buriti2Nelson Jorge Schuch3Space and Atmospheric Sciences Division, Physical Research LaboratoryAeronomy Division, National Institute for Space Research (INPE)Federal University of Campina GrandeSouthern Regional Space Research Center-CRS/COCRE/INPE-MCTICAbstract The characteristic features of the quarterdiurnal tide (QDT) in the mesosphere and lower thermosphere (MLT) are investigated using meteor radar observations from three low-latitude southern hemispheric stations, Sao Joao do Cariri (7.4°S, 36.5°W), Cachoeira Paulista (22.7°S, 45°W) and Santa Maria (29.7°S, 53.7°W) in 2005. The QDT shows consistent appearance with a weak enhancement during late summer and fall interval. The QDT amplitudes are found to be much smaller (< 3 m/s) than the longer period tidal components most of the times of the year consistent with the previous investigations carried out from various locations over the globe. The vertical wavelength is found to reach up to 80 km in the MLT maximizing in winter although most of the times it remains within 20 km. Therefore, based on the observed characteristics of the QDT, it is surmised that both the migrating and nonmigrating components are involved in manifestation of the QDT at present locations. Further detailed investigations are sought in connection with the important issues pertained to the actual excitation mechanisms and existing dominant QDT modes in the low-latitude MLT.http://link.springer.com/article/10.1186/s40623-018-0910-9Quarterdiurnal tideMesosphere and lower thermosphereMeteor radar observations
collection DOAJ
language English
format Article
sources DOAJ
author Amitava Guharay
Paulo Prado Batista
Ricardo Arlen Buriti
Nelson Jorge Schuch
spellingShingle Amitava Guharay
Paulo Prado Batista
Ricardo Arlen Buriti
Nelson Jorge Schuch
On the variability of the quarter-diurnal tide in the MLT over Brazilian low-latitude stations
Earth, Planets and Space
Quarterdiurnal tide
Mesosphere and lower thermosphere
Meteor radar observations
author_facet Amitava Guharay
Paulo Prado Batista
Ricardo Arlen Buriti
Nelson Jorge Schuch
author_sort Amitava Guharay
title On the variability of the quarter-diurnal tide in the MLT over Brazilian low-latitude stations
title_short On the variability of the quarter-diurnal tide in the MLT over Brazilian low-latitude stations
title_full On the variability of the quarter-diurnal tide in the MLT over Brazilian low-latitude stations
title_fullStr On the variability of the quarter-diurnal tide in the MLT over Brazilian low-latitude stations
title_full_unstemmed On the variability of the quarter-diurnal tide in the MLT over Brazilian low-latitude stations
title_sort on the variability of the quarter-diurnal tide in the mlt over brazilian low-latitude stations
publisher SpringerOpen
series Earth, Planets and Space
issn 1880-5981
publishDate 2018-08-01
description Abstract The characteristic features of the quarterdiurnal tide (QDT) in the mesosphere and lower thermosphere (MLT) are investigated using meteor radar observations from three low-latitude southern hemispheric stations, Sao Joao do Cariri (7.4°S, 36.5°W), Cachoeira Paulista (22.7°S, 45°W) and Santa Maria (29.7°S, 53.7°W) in 2005. The QDT shows consistent appearance with a weak enhancement during late summer and fall interval. The QDT amplitudes are found to be much smaller (< 3 m/s) than the longer period tidal components most of the times of the year consistent with the previous investigations carried out from various locations over the globe. The vertical wavelength is found to reach up to 80 km in the MLT maximizing in winter although most of the times it remains within 20 km. Therefore, based on the observed characteristics of the QDT, it is surmised that both the migrating and nonmigrating components are involved in manifestation of the QDT at present locations. Further detailed investigations are sought in connection with the important issues pertained to the actual excitation mechanisms and existing dominant QDT modes in the low-latitude MLT.
topic Quarterdiurnal tide
Mesosphere and lower thermosphere
Meteor radar observations
url http://link.springer.com/article/10.1186/s40623-018-0910-9
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